The present Geological Survey of the United States was organized in 1879. In 1880, in connection with the Colorado work, a chemical laboratory was established at Denver in charge of W. F. Hillebrand, with whom were associated Antony Guyard and, later, L. G. Eakins. In 1882 W. H. Melville was placed in charge of a second laboratory at San Francisco, and in the autumn of 1883 the central laboratory was started in Washington, with myself as chief chemist. In November, 1885, Dr. Hillebrand was transferred to Washington; early in 1888 he was followed by Mr. Eakins, and the Denver laboratory was discontinued. In the spring of 1890 Dr. Melville also was transferred to Washington, and since then the geochemical work of the Survey has been concentrated at headquarters. The special laboratories of the water-resources and technologic branches of the Survey are not included in this statement and their work is not represented in this bulletin.
Up to January 1, 1914, nearly 8,000 analyses have been made in the laboratory at Washington of rocks, minerals, ores, waters, sediments, coals, metals, and other substances with which geology has to do. Some-hundreds of analyses were also made in the laboratories at Denver and San Francisco. A fair amount of research work upon mineralogical and analytical problems has also been done. In *all of this work the following chemists have been employed: E. T. Allen, R. K. Bailey, Charles Catlett, T. M. Chatard, F. W. Clarke, L. G. Eakins, J. G. Fairchild, F. A. Gooch, Antony Guyard, W. B. Hicks, W. F. Hillebrand, W. F. Hunt, W. H. Melville, H. C. McNeil, Chase Palmer, R. B. Riggs, W. T. Schaller, E. A. Schneider, George Steiger, H. N. Stokes, E. C. Sullivan, William Valentine, R. C. Wells, W. C. Wheeler, and J. E. Whitfield. At present, January 1, 1914, eight of these chemists are employed in the Survey. Other officers of the Survey have been occupied more or less with chemical questions, but the men named in this list were connected directly with the laboratory. Some work for the chemical division has also been done by chemists not regularly on the rolls of the Survey, but their analyses, with the exception of a single group to be noted later, do not fall within the scope of this paper.
No abstract available.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp345B","usgsCitation":"Schwennesen, A., and Meinzer, O.E., 1915, Ground water for irrigation in the vicinity of Enid, Oklahoma, with a note on ground water for irrigation on the Great Plains: U.S. Geological Survey Water Supply Paper 345, 13 p., https://doi.org/10.3133/wsp345B.","productDescription":"13 p.","startPage":"11","endPage":"23","costCenters":[],"links":[{"id":422349,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24517.htm","linkFileType":{"id":5,"text":"html"}},{"id":264416,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0345b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264417,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0345b/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","city":"Enid","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -98.107,\n 36.589\n ],\n [\n -98.107,\n 36.243\n ],\n [\n -97.643,\n 36.243\n ],\n [\n -97.643,\n 36.589\n ],\n [\n -98.107,\n 36.589\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dbbf","contributors":{"authors":[{"text":"Schwennesen, A.T.","contributorId":83511,"corporation":false,"usgs":true,"family":"Schwennesen","given":"A.T.","affiliations":[],"preferred":false,"id":149739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":887469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70179606,"text":"70179606 - 1914 - Progress report on stream measurement work carried on in cooperation with the United States Geological Survey: Section in Ninth biennial report of the State Engineer to the governor of Utah: 1913-1914","interactions":[],"lastModifiedDate":"2017-01-24T11:07:45","indexId":"70179606","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1914","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5276,"text":"Utah State Engineer Biennial Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Progress report on stream measurement work carried on in cooperation with the United States Geological Survey: Section in Ninth biennial report of the State Engineer to the governor of Utah: 1913-1914","docAbstract":"Utah, like other states in the arid region of the United States, points with just pride to her present and future agricultural developments. She proudly boasts, and no doubt justly too, that her fields of green vegetation are inexhaustible and always expanding, and with due vigilance and care on the part of her land holders these fields will bring forth the proper supplies for man for an indefinite period. But, like her neighboring sister states on the east, west, north, and south, she realizes that the precipitation over her lands, as a general rule, is insufficient for the growing and maturing of crops. As a result, her principal lands can only be made to bear crops through the assistance of irrigation. In all irrigation, next to the land itself, the most important factor to be considered is the water supply.
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From the headwater\nregion, including Shoshone, Lewis, and Heart lakes, in Yellowstone\nNational Park, the river flows southward, broadening into\nJackson Lake (4 miles wide and 18 miles long) and passing through\nJackson Valley (8 miles wide and 40 miles long), beyond which, near\nthe Idaho-Wyoming line, it enters a long canyon. At the south\nedge of Madison County, Idaho, it receives Henrys Fork, below which\nthe Snake flows southward and westward across Idaho to a point\nnear Homedale, near the Oregon-Idaho line, where it turns abruptly\nnorthward and beyond which it forms for about 170 miles the boundary\nbetween Idaho and Oregon and for 30 miles more that between\nIdaho and Washington. It enters Washington at Lewiston, flows\nnorthwest, west, and southwest, and joins the Columbia near Pasco.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp347","collaboration":"Prepared under the direction of R. B. 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The maximum elevation\nof the upper rim of the basin is 13,000 feet above sea level.\nThe upper part of the basin comprises a rough, broken country,\nwell drained by numerous short streams, most of which are confined\nto steep, narrow canyons. The streams are fed by many small springs\nand by the melting of the snow which forms the greater part of the\nprecipitation. The rocks of the extreme headwater region are chiefly\nsandstones and quartzites and are covered with a thin layer of soil\nthat supports scattered groves of fir and aspen. A few small lakes\nlie near the head of the river.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp350","collaboration":"Prepared under the direction of R. B. 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